Atmospheric and radiometric correction is the basis and key for quantificational remote sensing. 卫星遥感数据的大气辐射校正是定量遥感的基础与关键。
The approach of surface temperature to estimate the spatial distribution of evapotranspiration by using remote sensing is very attractive. 摘要通过遥感方法反演表面温度来计算地表蒸散量是定量遥感的一个很有潜力的应用领域。
